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THIS HALF OF THE PRESENTATION:
An overview of NCAR ACOM ‘process studies’ activities Topics, Activities and Problems in Gas-phase Atmospheric Chemistry Autoxidation Organic Nitrates Chemistry of Oxygenates and Multifunctional Species Aromatics – esp. oxygenated, wildfire emissions… Others… Kelley will follow with a perspective on condensed phase chemistry topics / questions
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10 m3 Teflon Bag (Zhang et al., AMT, 2018)
NCAR ‘Big Chamber’ 10 m3 Teflon Bag (Zhang et al., AMT, 2018) NO3- TOF-CIMS, PTR-MS, GC-FID, … Amenable to inclusion of additional instrumentation Focusing on continuous-flow mode Low, steady-state NOx conditions Early focus - OH and NO3 Isoprene Oxidation experiments Oxygenated aromatics (wildfire emissions) NO3-initiated oxidation of BVOC Xuan Zhang
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50 L stainless steel, T-regulated (220-350 K) FTIR, GC-FID
NCAR ‘Little Chamber’ 50 L stainless steel, T-regulated ( K) FTIR, GC-FID Amenable to inclusion of additional instrumentation (TOGA, PTR-MS, CIMS, CEAS, HPLC, …) No-cost collaborators on multiple NSF proposals Oxidation of organics by OH, NO3, O3, Cl, Br Relative rate studies Mechanistic studies (end-products) Alkoxy, peroxy radical reaction pathways Nitrate production from RO2/NO reactions (poster) OH site of attack on oxygenates / multi-functionals Geoff Tyndall
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GECKO-A Generator for Explicit Chemistry and Kinetics of Organics in the Atmosphere INITIALIZE: Data base of laboratory measurements, for the most part evaluated critically PROCESS: Molecular structure parser Structure-Activity Relations (SARs) Estimate: kinetics, products, and their properties, e.g.: thermal and photolysis rxns explicit molecular structures enthalpy DH, vapor pressure Psat, Henry’s law Hsol, spectra s(l) Recursive: VOCs OVOCs CO2, H2O OUTPUT: Detailed chemical mechanism, species, and their properties POST-PROCESSING: Box model: Emissions & deposition, photo-chemistry, dilution/ventilation, evolving BL height,…, Simulate: Chambers, PBLs, Lagrangian parcels… SOME APPLICATIONS: Detailed atomic and molecular budgets Indicator Ratios, e.g. O/C, N/C, OH reactivity, PAM Systematic mechanism reduction SOA yields (good agreement in chambers, improved in field) Condensed phase chemistry (clouds, aq. Aerosols) Sasha Madronich a-pinene oxidation (t = 5t) Cloud Aqueous phase Organic Particle NB: Next version of Leeds MCM will be derived from GECKO-A
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Process Studies of Clouds and Chemistry
Lightning (NOx) Removal via Precipitation Thunderstorm Effects on Composition Analyzing DC3 observations with WRF-Chem modeling Mary Barth Aqueous-Phase Chemistry Mary Barth, Ann Marie Carlton, Sara Lance Goal: To design a coordinated investigation of the effect of clouds on tropospheric composition Activities: Pilot Study: CPOC (Lance poster) Cloud Water Sampling Box Model Intercomparison (Barth poster) PBL transport NCAR LES with Chemistry
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Leads to multiple functional groups in one generation
AUTOXIDATION: (Perrin et al., 1998; Orlando, 2007; Peeters et al., 2009; Crounse et al., 2011,2013; Ehn et al., 2014; Wang and Wang, 2016; Wang et al., 2017’ Barsanti et al., 2017; Praske et al., 2018 …etc.) A unimolecular reaction involving H-atom transfer in an organic peroxy radical: Leads to multiple functional groups in one generation
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Reverse reaction usually MUCH faster than forward.
AUTOXIDATION: (Perrin et al., 1998; Orlando, 2007; Peeters et al., 2009; Crounse et al., 2011, 2013; Ehn et al., 2014; Wang and Wang, 2016; Wang et al., 2017; Barsanti et al., 2017; Praske et al., 2018 …etc.) A unimolecular reaction involving H-atom transfer in an organic peroxy radical: Typically endothermic, thus strongly T-dependent; factor of 10 in rate for 25 K. Reverse reaction usually MUCH faster than forward. Often the first isomerization sets the stage for more.
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AUTOXIDATION: (what goes around, might go around again and again)
RO2 lifetime against bimolecular reactions for different [NO]: 10 ppt NO 100 s ppb NO 0.4 s Lots of time in the background atmosphere (minutes); as we lower NOx, increasing amount of time (seconds) in urban / suburban locations. (Praske et al., 2018) Lots of likely possibilities – biogenics, especially pristine conditions (Peeters, Crounse, Ehn) But anthropogenic too! Alkane chemistry, ethers, alcohols, aldehydes, hydroperoxides, aromatics – any weak-ish C-H bonds in appropriate places. What do we need to do (already happening) – Use combination of lab and theory to develop quantitative knowledge of rates of these processes (SARs) for incorporation into mechanisms.
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ORGANIC NITRATES: Formation and loss can control NOx distributions and lifetimes (hence ozone) (e.g., Ayres et al., 2015; Romer et al., 2016; Ebben et al., 2017) Permanent sinks or temporary reservoirs? Peroxy Radical reactions with NO: Still work to do, formation and loss, even for simple systems (alkanes, alkenes), but especially for functionalized peroxy radicals.
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ORGANIC NITRATES: NO3 Reactions with Unsaturated species (Biogenics): Many studies on NO3 / monoterpene reactions, in particular as sources of SOA. Ng et al., ACP 2017 Need to understand peroxy radical fate and chemistry, losses of nitrates by photoxidation, hydrolysis, etc., … Lots of work being done here (Fry et al., 2014; Boyd et al., 2015, 2017; Slade et al., 2017; Faxon et al., 2018; Claflin and Ziemann, 2018…) Kurten et al., 2017: Subtle changes in structure different behavior of an alkoxy species v. different SOA yields.
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CHEMISTRY OF MULTI-FUNCTIONAL ORGANICS:
Chemistry of Dodecane in GECKO-A Increased Functionalization = more uncertainty in lifetime, ‘site-of-attack’, outcome.
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Can we judiciously select the most relevant compounds for study (rate coefficients and site-of-attack) so as to understand effects of multiple substituents, extend the utility of SARs, and develop predictive power for multifunctionals? CHEMISTRY OF MULTI-FUNCTIONAL ORGANICS: Chemistry of Dodecane in GECKO-A Increased Functionalization = more uncertainty in lifetime, ‘site-of-attack’, outcome. NB: “Volatile chemical products”, too (McDonald et al., 2018; Khare and Gentner, 2018)
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CHEMISTRY OF FURANS / OXYGENATED AROMATICS FROM BIOMASS BURNING:
Obviously, a large focus on biomass burning right now WE-CAN about to happen, NSF C-130, E. Fischer (CSU). FIREX-AQ – NASA/NOAA, Summer 2019 FIRELAB experiments (e.g., Stockwell et al., 2015; Hatch et al., 2017; Koss et al., 2018) – hundreds of VOC identified / quantified Loosely speaking: product of emission strength, reactivity, SOA potential and unknowns in the chemistry points to a series of furans and oxygenated aromatic species… Lab studies needed – oxidative chemistry, SOA production, brown carbon (Sangwan and Zhu, 2018; Finewax et al., 2018, …)
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COULD HAVE DISCUSSED MANY OTHERS:
Criegee radical chemistry – lots of activity, driven by direct detection and potential importance as sulfate source (Mauldin et al., 2012; Welz et al., 2012; Nguyen et al., 2016; Taatjes, 2017; Enami et al., 2017; Vereecken et al., 2017, …). Halogens – everything from Arctic, MBL in general, Hg chemistry, global tropospheric ozone, to urban regions. Terpene Oxidation in general (OH/O3) – reactive, SOA sources, lots of activity; field missions coming (COALA-BAIR). What level of detail do we require, how do we best achieve that? HOx budgets in multiple locations. Are we there yet? Missing processes? Urban ‘high-NOx chemistry’?
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GECKO-A ‘hyper-explicit’ mechanism generator
Aircraft campaigns GECKO-A ‘hyper-explicit’ mechanism generator Earth System Models Aircraft instruments Fast GC/MS, CIMS Lab-based process studies
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